1994
DOI: 10.1029/94tc01502
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Rates of deformation, uplift, and landscape development associated with active folding in the Waipara area of North Canterbury, New Zealand

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Cited by 34 publications
(40 citation statements)
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“…This conclusion is unexpected, considering the high proportion of plate boundary strain that is associated with the Marlborough fault system (Lamb & Bibby 1989), and is different from the Wellington region where Ota et al ( 1981 ) found the strike-slip faults of southern North Island formed the boundaries to blocks on which the marine terraces were tilted and deformed. This conclusion, however, is similar to that of Nicol et al (1994) for the Waipara region of north Canterbury.…”
Section: Discussionmentioning
confidence: 39%
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“…This conclusion is unexpected, considering the high proportion of plate boundary strain that is associated with the Marlborough fault system (Lamb & Bibby 1989), and is different from the Wellington region where Ota et al ( 1981 ) found the strike-slip faults of southern North Island formed the boundaries to blocks on which the marine terraces were tilted and deformed. This conclusion, however, is similar to that of Nicol et al (1994) for the Waipara region of north Canterbury.…”
Section: Discussionmentioning
confidence: 39%
“…1), and movement on this fault is inferred to be responsible for uplift and tilting of the peninsula. In contrast to the coincidence ( > in deformation pattern of the interglacial terraces and underlying Tertiary folds near Cape Campbell described above, and the Waipara area (Nicol et al 1994), there is no such correlation at Kaikoura Peninsula (Fig. 9), where a series of northeast-striking, short wavelength (1-2 km) folds disrupt the Upper Cretaceous -middle Miocene bedrock sequence.…”
Section: Kaikoura Peninsulamentioning
confidence: 67%
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“…1). From Mount Grey to the Waipara River mouth, the PPAFZ passes into the northeast-trending coastal folds which are locally rotated clockwise into an en echelon, sigmoidal pattern (Yousif 1985;Nicol et al 1994;Al-Daghastani & Campbell 1995). Cowan et al (1996) also incorporated the Lees Valley and Ashley faults as PPAFZ splays.…”
Section: Strike-slip Faultsmentioning
confidence: 99%
“…1), but step back to the coast near the Ashley River. Along-strike southwards migration of this west-facing system onshore leads to coastal uplift, with growing hills closing the Waipara basin from the sea during Otiran glacial times and tectonically induced Holocene uplift and progradation extending south to at least the Ashley River mouth (Yousif 1985;Nicol et al 1994;Al-Daghastani & Campbell 1995;Shulmeister & Kirk 1996;Dodson 2009). The progradation cycles identified by Shulmeister & Kirk (1996) are close to the dates for major range-front earthquakes inland (Howard et al 2005) and to episodic downcutting on the Waipara River, so may be a consequence of coseismic uplift.…”
Section: Introductionmentioning
confidence: 99%